{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,31]],"date-time":"2026-03-31T07:28:18Z","timestamp":1774942098324,"version":"3.50.1"},"reference-count":63,"publisher":"MDPI AG","issue":"11","license":[{"start":{"date-parts":[[2020,10,26]],"date-time":"2020-10-26T00:00:00Z","timestamp":1603670400000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100002261","name":"Russian Foundation for Basic Research","doi-asserted-by":"publisher","award":["20-35-70052"],"award-info":[{"award-number":["20-35-70052"]}],"id":[{"id":"10.13039\/501100002261","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100002261","name":"Russian Foundation for Basic Research","doi-asserted-by":"publisher","award":["19-29-05085"],"award-info":[{"award-number":["19-29-05085"]}],"id":[{"id":"10.13039\/501100002261","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100002261","name":"Russian Foundation for Basic Research","doi-asserted-by":"publisher","award":["19-05-00403"],"award-info":[{"award-number":["19-05-00403"]}],"id":[{"id":"10.13039\/501100002261","id-type":"DOI","asserted-by":"publisher"}]},{"name":"NIR","award":["0264-2019-0010"],"award-info":[{"award-number":["0264-2019-0010"]}]},{"name":"Institute of geology and mineralogy SB RAS","award":["State assignment"],"award-info":[{"award-number":["State assignment"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Water"],"abstract":"<jats:p>The article presents the studies on understanding the chemical evolution of Maloye Yarovoe lake that is located in the semi-arid landscape of and represent the most widespread chemical type of saline lake (Cl-Na) on the territory of Kulunda steppe (south of Western Siberia). The lake has gone through several changes in its state which are well represented in its sediments: section 1 (4.52\u20134.97 m) represents the subbase; section 2 (3.0\u20134.57 m) corresponds to a \u201cshallow lake\u201d stage and contains two sublayers; section 3 (0\u20132.25 m) illustrates an increase in erosion of the shoreline and corresponds to a \u201cdeep lake\u201d stage. The extrapolation of radiocarbon dates suggests that the most significant changes in the state of the lake occurred at about 6.5\u20137.1 ka BP (transition from a small lake to a large one with intensified coastal erosion) and at about 5.69 and 3.5 ka BP (increase in the organic component). The results of sequential extraction of elements correspond to chemical changes occurred in a certain time of the lake state by changing in their distribution level and fraction type along the core. The results of lake water evaporation and organic matter degradation modelling performed in Phreeqc for oxic and anoxic condition showed the following stages of chemical divides could be expected in case of further lakes desiccation: Halite\u2014Epsomite\u2014Bischofite\/Carnalite with possibility of Nahcolite precipitation in carbonate enriched periods (summer and autumn periods of organic matter degradation). Water\u2013rock interaction processes in combination with biogeochemical reactions affect drastically not only the migration features of elements in water and sediments, but also the type of mineral crystallization in lake sediments.<\/jats:p>","DOI":"10.3390\/w12113001","type":"journal-article","created":{"date-parts":[[2020,10,26]],"date-time":"2020-10-26T10:38:35Z","timestamp":1603708715000},"page":"3001","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":6,"title":["Distribution Profile of Chemical Elements during the Last 13 Thousand Years from the Sediments of Maloye Yarovoe Lake (Western Siberia, Russia)"],"prefix":"10.3390","volume":"12","author":[{"given":"Marina","family":"Kolpakova","sequence":"first","affiliation":[{"name":"Sobolev Institute of Geology and Mineralogy, SB RAS, 630090 Novosibirsk, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-3885-5015","authenticated-orcid":false,"given":"Olga","family":"Gaskova","sequence":"additional","affiliation":[{"name":"Sobolev Institute of Geology and Mineralogy, SB RAS, 630090 Novosibirsk, Russia"},{"name":"Novosibirsk State University, 630090 Novosibirsk, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Svetlana","family":"Borzenko","sequence":"additional","affiliation":[{"name":"Institute of Natural Resources, Ecology and Cryology, SB RAS, 672002 Chita, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Sergey","family":"Krivonogov","sequence":"additional","affiliation":[{"name":"Sobolev Institute of Geology and Mineralogy, SB RAS, 630090 Novosibirsk, Russia"},{"name":"Novosibirsk State University, 630090 Novosibirsk, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9133-5468","authenticated-orcid":false,"given":"Olga","family":"Naymushina","sequence":"additional","affiliation":[{"name":"Sobolev Institute of Geology and Mineralogy, SB RAS, 630090 Novosibirsk, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-1536-6470","authenticated-orcid":false,"given":"Natalia","family":"Rudaya","sequence":"additional","affiliation":[{"name":"Sobolev Institute of Geology and Mineralogy, SB RAS, 630090 Novosibirsk, Russia"},{"name":"Institute of Archaeology &amp; Ethnography, SB RAS, 630090 Novosibirsk, Russia"},{"name":"Biological Institute, Tomsk State University, 634000 Tomsk, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1968","published-online":{"date-parts":[[2020,10,26]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"810","DOI":"10.1038\/nclimate3111","article-title":"Earth\u2019s surface water change over the past 30 years","volume":"6","author":"Donchyts","year":"2016","journal-title":"Nat. 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